摘要
贵州处于喀斯特地貌发育广泛的地区,在岩溶地貌广泛发育的背景下,地下水以各种形式存在于地下岩溶裂隙空间中。研究显示,乌当区北部地下水多以溶蚀孔隙的裂隙水为主,溶蚀溶洞的裂隙水次之,地下水出露点分布较广,向低洼区分布且区域分散,出水量较少导致取水难度大。根据乌当区北部地下水特征对其进行利用开发给出合理建议。
Guizhou has large area of karst landform,and groundwater resources are abundant here. Researches showed that in the northern part of Wudang District,groundwater mainly existed in corrosion pores and corrosion caves. The emergence points of groundwater distributed widely in low-lying areas,and were scattered with little water yield,thus increasing the difficulty of exploitation. According to the characteristics of groundwater in the northern part of Wudang District,we put forward some advices for the exploitation and utilization of groundwater in this area.
作者
张育林
程星
王恒松
张祥祥
吴伟
张辉华
ZHANG Yulin;CHENG Xing;WANG Hengsong;ZHANG Xiangxiang;WU Wei;ZHANG Huihua(School of Geography and Environmental Science,Guizhou Normal University,Guiyang 550025,China;State Engineering Technology Institute for Karst Desertification Control,School of Karst Science,Guizhou Normal University, Guiyang 550001,China;Liping County State-owned Shijingshan Forest Farm,Liping 557300,China)
出处
《贵州科学》
2018年第6期74-80,共7页
Guizhou Science
关键词
乌当区北部
地下水
地下水开发利用研究
the northern part of Wudang District
groundwater
groundwater exploitation and utilization research